Abstract
In Tunisia, the Mejerda basin is the most important agricultural sector. Identification of additional water sources and good management of current and new resources is required to maintain and increase its productivity. The present study concerns the Ariana region (north-east of Tunisia) covering the eastern part of Mejerda basin. Lithological columns, well logs, vertical electrical soundings, and gravity data were analyzed and interpreted to give more precise information for exploitation of the water resources of the Ariana region. Lithological columns, well logs, and geoelectrical models reveal that the permeable Quaternary alluvial deposits, the Upper Campanian–Lower Maestrichtian, Albian and Barremian limestones, and Valanginian–Hauterivian sandstones are the main aquifers in Ariana. Comparison of geoelectrical cross sections to the Bouguer anomaly map of the Ariana region reveals tectonic influence on the geometry of the aquifers. The folded structures attributed to the Tortonian compressive stress and the tectonic movements in N–S, E–W, NW–SE, and NE–SW directions have resulted in the compartmentalization of Ariana’s aquifers into subsided and raised blocks. This reconstituted geometry of the region influenced the depth of burial of permeable lithologies and inhibited groundwater circulation in some localities.
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Amiri, A., Chaqui, A., Hamdi Nasr, I., Inoubli, M. H., Ben Ayed, N., & Tlig, S. (2011). Role of preexisting faults in the geodynamic evolution of Northern Tunisia, insights from gravity data from the Medjerda valley. Tectonophysics, 506, 1–10.
Asfahani, J. (2006). Geoelectrical investigation for characterizing the hydrogeological conditions in semi-arid region in Khanasser valley, Syria. Journal of Arid Environments, 68, 31–52.
Ben Ayed, N. (1986). Evolution tectonique de l’avant pays de la chaine alpine de la Tunisie du début du mésozoïque à l’actuel. Thèse es- Sciences, Univ. Paris Sud, centre Orsay, pub.
Benassi, R., Jallouli, C., Hammami, M., & Turki, M. M. (2006). The structure of Jebel El Mourra, Tunisia: A diapiric structure causing a positive gravity anomaly. Terra Nova, 18, 432–439.
Blakely, R., & Simpson, R. (1986). Approximating edges of source bodies from magnetic or gravity anomalies. Geophysics, 51, 1494–1498.
Briggs, I. (1974). Machine contouring “using minimum curvature”. Geophysics, 39, 39–48.
Chapellier, D. (1992). Well logging in hydrogeology. Brook field, MA: A.A. Balkema Publishers.
Cordell, L. (1979). Gravimetric expression of graben faulting in Santa Fe Country and the Espanola Basin. In New Mexico Geological Society Guidebook, 30th Field Conference (pp. 59–64), New Mexico.
Cordell, L., & Grauch, V. J. S. (1985). Mapping basement magnetization zones from aeromagnetic data in the San Juan Basin, New Mexico. In W. J. Hinze (Ed.), The utility of the regional gravity and magnetic anomaly maps (pp. 181–197). Tulsa, OK: Society of Exploration Geophysicists.
Cudennec, C., Leduc, C., & Koutsoyiannis, D. (2007). Dryland hydrology in Mediterranean regions review. Hydrogeological Sciences Journal, 52, 1077–1087.
Desbrandes, R. (1968). Théorie et interprétation des diagraphies. Paris: Publications de l’institut Français du Pétrole.
Ellis, D.V., & Singer, J.M. (2007). Well logging for earth scientists. New York: Springer. ISBN: 1401037384.
Gouasmia, M., Gasmi, M., Mhamdi, A., Bouri, S., & Ben Dhia, H. (2006). Prospection géoéléctrique pour l’étude de l’aquifère thermal des calcaires récifaux Hmeima-Boujaber (Centre ouest de la Tunisie). Comptes rendus des Géosciences, 338, 1219–1227.
Guellala, R., Ben Marzoug, H., Inoubli, M. H., & Moumni, L. (2011). Apports de la Sismique Réflexion à l’étude de l’aquifère du Continental Intercalaire du Jérid (Tunisie). Hydrological Sciences Journal, 5, 1040–1052.
Guellala, R., Inoubli, M. H., & Amri, F. (2009). Nouveaux éléments sur la structure de l’aquifère superficiel de Ghardimaou (Tunisie): contribution de la géophysique électrique. Hydrological Sciences Journal, 54, 974–983.
Hamdi Nasr, I., Ben Salem, A., Inoubli, M. H., Dhifi, J., Alouani, R., Chaqui, A., et al. (2008). Apports de la gravimétrie dans la caractérisation des structures effondrées dans la région de Nebeur (Nord Ouest de la Tunisie). Swiss Journal of Geosciences, 101, 17–27.
Hearst, J.R., & Nelson, P.H. (1985). Well logging for physical properties. New York: McGraw-Hill. ISBN 0070276986.
Hsieh, B. Z., Lewis, C., & Lin, Z. S. (2005). Lithology identification of aquifers from geophysical well logs and fuzzy logic analysis: Shui-Lin Area, Taiwan. Computers & Geosciences Journal, 31, 263–275.
Jallouli, C., & Mickus, K. (2000). Regional gravity analysis of the crustal structure of Tunisia. Journal of African Earth Sciences, 30, 63–78.
Jauzein, A. (1967). Notice de la feuille 13 de l’Ariana. Tunis: Service géologique de Tunisie.
Jenny, J. & Borreguerro, M. (1993). WINSEV, programme d’interprétation des sondages électriques verticaux réalisés selon le dispositif Schlumberger. W-Geosoft.
Jouirou, M. (1982). Faciès sédimentaires et processus dynamiques dans la formation d’un milieu lagunaire: Evolution holocène et actuelle du lac de Tunis et de ses abords. Thèse de Doctorat, Université de Bordeaux I.
Kacem, J. (2004). Etude sismotectonique et évaluation de l’Aléas sismique régional du Nord-Est de la Tunisie: Apport de la sismique réflexion dans l’identification des sources sismogeniques. PhD thesis, Université Tunis II.
Keller, G.V., & Frischknecht, F.C. (1982). Electrical methods in geophysical prospecting. Oxford: Pergamon Press.
Khattach, D., Keating, P., Mili, M., Chennouf, T., Andreieux, P., & Milhi, A. (2004). Apport de la gravimétrie à l'étude de la structure du bassin de Triffa (Maroc nord–oriental): Implications hydrogéologiques. Comptes Rendus Géosciences, 336, 1427–1432.
Kleh, M., Eichorst, F., & Schafer, A. (2002). Facies interpretation from wells logs applied to the tertiary lower Rhine basin fill. Netherlands Journal of Geosciences, 2, 167–176.
Lajmi, T., Biely, A., & Pini, S. (1971). Carte géologique de la région d’Ariana; feuille n° 13.
Maamri, R. (1998). La fracturation et ses conséquences sur les risques sismiques et naturels de la région de Tunis. DEA, Université de Tunis.
Najine, A., Jaffal, M., El Khammari, K., Aïfa, T., Khattach, D., Himi, M., et al. (2006). Contribution de la gravimétrie à l’étude de la structure du bassin de Tadla (Maroc): Implications hydrogéologiques. Comptse rendus des Geosciences, 338, 676–682.
ONM (2001). Campagne gravimétrique CG4. Coupures 1/50 000 de Ariana, Tunis, Marsa et Gamaret.
Pertu, N., Wattanasen, K., Phommasone, K., & Elming, S. (2011). Characterization of aquifers in Vientiane Basin, Laos, using magnetic resonance sounding and vertical electrical sounding. Journal of Applied Geophysics, 73, 207–220.
Pini, S. (1966). Notice explicative de la feuille 13 de l’Ariana. Tunis: Service géologique.
Prieto, C. (1996). Gravity/magnetic signatures of various geologic models—An exercise in pattern recognition. IGC Footnote Series, 4(4), 1–24.
Rapti-Caputo, D., Bratus, A., & Santarato, G. (2009). Strategic groundwater resources in the Tagliamento River basin (northern Italy): Hydrogeological investigation integrated with geophysical exploration. Hydrogeology Journal, 17, 1393–1409.
Rider, M.H. (1986). The geological interpretation of wells logs. Blackie: Halsted Press. ISBN: 0470202815.
Sarsar Naouali, B., Hamdi Naser, I., Amiri, A., Chaqui, A., & Inoubli, M.H. (2010). Gravity data as a tool for delineating subsurface geology of Ariana region (Diapir zone, Tunisia). EGM 2010 International Workshop: Adding New Value to Electromagnetic, Gravity and Magnetic Methods for Exploration, Expanded Abstracts.
Sarsar Naouali, B., Inoubli, M. H., Amiri, A., Chaqui, A., & Hamdi, I. (2011). Subsurface geology of the Ariana region (Diapir zone, northern Tunisia) by means of gravity analysis. European Association of Geoscientists & Engineers, Geophysical Prospecting, 59, 983–997.
Sebei, K., Inoubli, M. H., Boussiga, H., Tlig, S., Alouani, R., & Boujamaoui, M. (2007). Seismic stratigraphy, tectonics and depositional history in the Halk el Menzel region, NE Tunisia. Journal of African Earth Sciences, 47, 9–29.
Serra, O. (1984). Fundamentals of well log interpretation. The acquisition of logging data. Amsterdam: Elsevier. ISBN: 0444416250.
Schoeffler, J. (1975). Gravimétrie appliquée aux recherches structurales et à la prospection pétrolière et minière (p. 288). Technip, Paris.
Telford, W. M., Geldart, B. P., & Sheriff, R. E. (1976). Applied geophysics. London: Cambridge University Press.
Tizro, A. T., Voudouris, K. S., Salehzade, M., & Mashayekhi, H. (2010). Hydrogeological framework and estimation of aquifer hydraulic parameters using geoelectrical data: A case study from West Iran. Hydrogeology Journal, 18, 917–929.
Truillet, R., & Turki, M. M. (1980). La tectonique tangentielle dans la zone des diapirs. L’exemple de Djebel Ammar (Tunisie septentrionale). Comptes rendus de l’académie des sciences, 291, 325–327.
Zouhri, L. (2001). L’aquifere du bassin de la Mamora, Maroc: géométrie et écoulement souterrains (Aquifer of the Mamora basin, Morocco: geometry and groundwater flow). Journal of African Earth Sciences, 32, 837–850.
Zouhri, L., Gorini, C., Mania, J., Deffontaines, B., & Zerouali, A. (2004). Spatial distribution of resistivity in the hydrogeological systems, and identification of the catchment area in the Rharb basin, Morocco. Hydrological Sciences Journal, 49(3), 387–398.
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The authors are indebted to Dr. John Carranza and anonymous reviewers for their comments, constructive criticism, and corrections which helped to improve the original version of this manuscript.
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Ben Lasmar, R., Guellala, R., Sarsar Naouali, B. et al. Contribution of Geophysics to the Management of Water Resources: Case of the Ariana Agricultural Sector (Eastern Mejerda Basin, Tunisia). Nat Resour Res 23, 367–377 (2014). https://doi.org/10.1007/s11053-014-9228-x
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DOI: https://doi.org/10.1007/s11053-014-9228-x